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RB 81/00114 Structural and metamorphic controls on the origin of nephrite jade near Cowell, SA.
1 of the worlds principal nephrite jade deposits was formed during a late phase tectonic event, involving cross-warping and fracturing of high grade metamorphic complex.-
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Published: 01 Nov 1981
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RB 89/00004 Cowell Jade - Talk presented at International Symposium on Geochemistry and Mineralization of Proterozoic Mobile Belts, Tianjin, China, September, 1988.
The talk Cowell jade : a Middle Proterozoic, marble-hosted, nephrite jade deposit gives a brief overview of previous compilations (quality, production, reserves, history, geology, structure, metamorphism, metasomatism and mechanism of nephrite...-
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Published: 01 Oct 1988
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RB 88/00054 Cowell Jade - A middle Proterozoic, marble-hosted, nephrite jade deposit.
Brief review of the deposit is presented, including regional geology, ore deposit features, production, history, quality, value, reserves and mining methods. It is the largest known high quality nephrite jade deposit in the world.-
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Published: 01 Jul 1988
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Cowell Jade Province: rock sample petrographic descriptions.
A collection of Amdel petrographic reports providing raw data for a petrogenetic study of Cowell area jade specimens and related host rocks carried out by SADME, aimed at determining geological controls on the distribution of high quality nephrite...-
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Published: 01 Jan 1990
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Gilles Downs (part of the Northern Eyre Peninsula Project). First annual report (prior to start of joint reporting status) for the period 8/7/2005 to 7/7/2006: and final report submitted at licence full surrender, for the succeeding period to 30/7/2015.
A licence area consisting of two separate sub-blocks located on the plains extending to the west of the Middleback Range on north-eastern Eyre Peninsula was taken up to explore for possible economic buried deposits of stratabound magnetite iron ore...-
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Data release - as updated : Moonabie (part of the East Eyre Peninsula Project). Annual reports plus final report to licence expiry/full surrender, for the period 1/5/2006 to 13/3/2017.
A licence consisting of three separate sub-blocks that are centred approximately 60 km WSW of Whyalla is being explored for possible economic primary uranium mineralisation plus precious and base metals, in a structurally complex epithermal and...-
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Published: 29 Apr 1917
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RB 2001/00006 Reconnaissance sampling of basement rocks of the Gawler Craton, South Australia, for dimension stone.
Eighty-five sites of crystalline basement rocks on the Gawler Craton were inspected to determine which lithological or stratigraphical units have potential for use as dimension stone. The Gawler Craton contains a variety of rock types including...-
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Published: 01 Oct 2000
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RB 2016/00001 SHRIMP U-Pb geochronology data for northern Eyre Peninsula, 2014–2016.
As part of the current mapping programme aiming to produce a second edition of the PORT AUGUSTA 1:250k geological map sheet, 8 rock samples from outcrops located on this map sheet area and on the adjoining WHYALLA 1:250k map sheet area were...-
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Published: 01 May 2017
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SADME/Amdel Project 1/1/186 : Geochronology of the ancient basement rocks of the Gawler Craton. Progress reports 1 to 24 for the period September 1976 to February 1982.
There is no abstract created for this record-
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Published: 01 Jan 1982
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Pinerow. Annual and final reports to licence expiry/full surrender for the period 2/10/2004 to 9/11/2008.
To continue the assessment of the dimension stone and ornamental stone potential of granitic basement outcrops present on EL 2851, a 5-year Retention Lease, RL 116, was taken out on 7/2/2006 to cover 5.9 ha of the Middle Camp granite pluton. Several...-
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Published: 08 Jan 1909
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Lake Gilles. Progress reports, annual reports and final report to licence full surrender, for the period 3/6/1991 to 16/4/1996.
Exploration for possible buried stratabound base metal deposits within Hutchison Group metasediments east of Kimba comprised an airborne magnetic-radiometric survey, ground magnetic surveys, RC drilling (338 holes, total 14,663 m) and one 279 m deep...-
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